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The Bridge River area is one of British Columbia’s oldest gold camps. Production commenced in 1858 when placer gold was recovered from Bridge River, near its confluence with the Fraser River. The placer gold was followed upstream from the Fraser, and in 1859, a second discovery was made on Gun Creek, near its confluence with the Bridge River, close to the (then) future site of the Minto Mine. Extensive placer operations were also initiated on Tyaughton and Hurley Rivers and on Cadwallader Creek. It wasn’t until the late 1800’s, however, that an interest emerged in identifying the placer source. This lead to the discovery of the Bralorne and the Pioneer deposits near the turn of the century. The Bralorne Mine became the largest gold producer in the region, yielding over 2.8 million ounces of gold and over 7 million ounces of silver. The Pioneer Mine, south of the Bralorne, and situate along the same greenstone belt, produced over 1.3 million ounces of gold and 25 million ounces of silver.
BRIDGE RIVER GOLD DISTRICT “RUSTY BUCK ”
MINFILE No 092JNE040 SUMMARY NMI Name RHODES Mining Division Lillooet BCGS Map 092J079 Status Showing NTS Map 092J16E Latitude 50º 45' 20" N UTM 10 (NAD 83) Longitude 122º 13' 30" W Northing 5622929 Easting 554666 Commodities Gold, Silver, Copper Deposit Types Tectonic Belt Intermontane Terrane Plutonic Rocks, Bridge River
Capsule Geology The Rhodes vein prospect, 0.6 kilometres east of Mission Pass, is at the contact between a body of granodiorite, presumably related to the Eocene Mission Ridge pluton, and sedimentary rocks, presumably of the Mississippian to Jurassic Bridge River Complex (Group). The prospect consists of pyrite, pyrrhotite and small amounts of chalcopyrite, within the intrusive margin of the granodiorite, and may represent a contact-replacement or skarn type mineralization. No further information is available on this particular showing, although similar mineralization exists at the King (092JNE126). These may in fact overlap the original Rhodes group of claims. A representative sample assayed 11.66 grams per tonne gold and 29.48 grams per tonne silver (Geological Survey of Canada Summary Report 1912, page 207).
Bibliography EMPR FIELDWORK 1974, p. 35; 1985, pp. 303-310; 1986, pp. 23-29; 1987, pp. 93-130; 1988, pp. 105-152; 1989, pp. 45-72; 1990, pp. 75-83 EMPR OF 1987-11; 1988-3; 1989-4; 1990-10 GSC OF 482 GSC P 77-2, p. 16 GSC SUM RPT *1912, p. 207
BRIDGE RIVER GOLD PROPERTY No. 2 “IN BETWEEN”
(AKA Moha) Tenure # 537697 Features - Quartz vein with 7.75g/t native Gold & 2.58g/t Silver ![]() Central coordinate: 122° 10’ 01.1” W Longitude, 50° 51’ 37.1” N Latitude The “In Between” tenure, a one cell claim comprising 20.398 hectares, is situate along Bridge River at Horseshoe Bend. Prospecting conducted over the tenure area during the mid 1930’s led to the discovery of a quartz vein bearing native gold. A low-tonnage bulk sample was taken, which assayed high gold values, however, low gold prices which followed the Great Depression of the 30’s, then the War years, coupled with further low gold prices, resulted in the property not being developed. GPEX conducted considerable research into the potential of this property, which resulted in its 2006 staking of the tenure. Only limited work has prevailed.
Access to the property is via the Bridge River Road, with the claim lying in the immediate vicinity of the famed Horseshoe Bend, approximately 24.1 road kilometres (20.25 air kilometres) northwest of Lillooet. The property is conducive to prospecting for about eight months out of the year.
This tenure is suited for continued exploration and development, or as a capital investment property.
MINFILE No 092JNE083
SUMMARY NMI Name MOHA Mining Division Lillooet BCGS Map 092J090 Status Prospect NTS Map 092J16E Latitude 50º 51' 35" N UTM 10 (NAD 83) Longitude 122º 10' 00" W Northing 5634556 Easting 558650 Commodities Gold, Silver Deposit Types I01 : Au-quartz veins Tectonic Belt Coast Crystalline Terrane Bridge River
Capsule Geology The Moha prospect is on the southeast side of Bridge River, 0.8 kilometre southeast of the confluence of Yalakom River with Bridge River. The prospect covers a quartz vein 15 to 38 centimetres wide within fractured andesitic greenstone of the Mississippian to Jurassic Bridge River Complex (Group). The vein contains native gold; no sulphides have been reported. In 1935, 93 grams of gold and 31 grams of silver were recovered from 12 tonnes of vein material (Minister of Mines Annual Report Index 3).
Bibliography EMPR AR 1913-272; 1936-F63 EMPR FIELDWORK 1974, p. 35; 1985, pp. 303-310; 1986, pp. 23-29; 1987, pp. 93-130; 1988, pp. 105-152; 1989, pp. 45-72; 1990, pp. 75-83 EMPR INDEX 3-205 EMPR OF 1987-11; 1988-3; 1989-4; 1990-10 GSC OF 1990-10 GSC SUM RPT *1933, Part A, p. 75
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